A simple model of the lowest layer of the atmosphere is developed for coupling to ocean models used to simulate sea surface temperature (SST). The model calculates the turbulent fluxes of sensible and latent heat in terms of variables that an ocean model either calculates (SST) or is forced by (winds). It is designed to avoid the need to specify observed atmospheric data (other than surface winds), or the SST, in the surface flux calculations of ocean models and, hence, to allow a realistic representation of the feedbacks between SST and the fluxes. The modeled layer is considered to be either a dry convective layer or the subcloud layer that underlies marine clouds. -from Authors
CITATION STYLE
Seager, R., Blumenthal, M. B., & Kushnir, Y. (1995). An advective atmospheric mixed layer model for ocean modeling purposes: global simulation of surface heat fluxes. Journal of Climate, 8(8), 1951–1964. https://doi.org/10.1175/1520-0442(1995)008<1951:AAAMLM>2.0.CO;2
Mendeley helps you to discover research relevant for your work.